| Type of Material: | Thesis |
| Title: | Air Sea Interaction processes over the Indo Pacific region and its impacts on Indian Ocean |
| Researcher: | Anil, Nisa |
| Guide: | Sajeev, R |
| Department: | Department of Physical Oceanography |
| Publisher: | Cochin University of Science & Technology, Cochin |
| Place: | Cochin |
| Year: | 2022 |
| Language: | English |
| Subject: | Air-Sea Interaction | Geosciences | Indian Ocean Dipole | Indo-Pacific Oceans | Ocean-Atmospheric Phenomena | Oceanography | Physical Sciences | Oceanography | Engineering and Technology |
| Dissertation/Thesis Note: | PhD; Department of Physical Oceanography, Cochin University of Science & Technology, Cochin, Cochin; 2022 |
| Fulltext: | Shodhganga |
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| 001 | 456349 | |
| 003 | IN-AhILN | |
| 005 | 2024-10-09 12:45:13 | |
| 008 | __ | 241009t2022||||ii#||||g|m||||||||||eng|| |
| 035 | __ | |a(IN-AhILN)th_456349 |
| 040 | __ | |aCUST_682022|dIN-AhILN |
| 041 | __ | |aeng |
| 100 | __ | |aAnil, Nisa|eResearcher |
| 110 | __ | |aDepartment of Physical Oceanography|bCochin University of Science & Technology, Cochin|dCochin|ein|0U-0253 |
| 245 | __ | |aAir Sea Interaction processes over the Indo Pacific region and its impacts on Indian Ocean |
| 260 | __ | |aCochin|bCochin University of Science & Technology, Cochin|c2022 |
| 300 | __ | |axvi, 186|dDVD |
| 502 | __ | |cDepartment of Physical Oceanography, Cochin University of Science & Technology, Cochin, Cochin|d2022|bPhD |
| 518 | __ | |d2023|oDate of Award |
| 518 | __ | |oDate of Registration|d2017 |
| 520 | __ | |aThe ocean and atmosphere are two interdependent systems. It is observed that a continuous exchange of heat, momentum, and freshwater between these two systems results in complex feedback loops. For a better understanding of the air-sea interaction processes, their mutual interaction must be examined thoroughly. The major coupled ocean-atmospheric phenomena in the Indo-Pacific regions are Indian Ocean Dipole (IOD) and the El-Niño Southern Oscillation (ENSO), respectively. The Indian Ocean is warmer in the eastern part and cooler in the western part, unlike the tropical Pacific and Atlantic Oceans. In some years, the Sea Surface Temperature Anomalies (SSTA) become alternately cooler over the eastern part and warmer over the western part of the equatorial Indian Ocean. This reversal in the SSTA between the eastern parts of Indian Ocean is termed as Indian Ocean Dipole (Saji et al., 1999). The intensity of IOD is determined by an index called Dipole Mode Index (DMI). This is the SSTA difference between western |
| 650 | __ | |aOceanography|2UGC |
| 650 | __ | |aEngineering and Technology|2AIU |
| 653 | __ | |aAir-Sea Interaction |
| 653 | __ | |aGeosciences |
| 653 | __ | |aIndian Ocean Dipole |
| 653 | __ | |aIndo-Pacific Oceans |
| 653 | __ | |aOcean-Atmospheric Phenomena |
| 653 | __ | |aOceanography |
| 653 | __ | |aPhysical Sciences |
| 700 | __ | |eGuide|aSajeev, R |
| 856 | __ | |uhttp://shodhganga.inflibnet.ac.in/handle/10603/529244|yShodhganga |
| 905 | __ | |afromsg |
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